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Published byEthel Ball Modified over 9 years ago
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Circulation in the atmosphere Circulation in the Atmosphere
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How does planetary rotation affect fluid motions? Additional forces in the rotating frame of reference –Centrifugal force Geoid –Coriolis force
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Coriolis force Exmaple: playing catch on a merry-go-round Straight path in inertial (non-rotating) frame Deflection to the right in rotating frame
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Coriolis force In northern hemisphere, planetary rotation is counter-clockwise. A moving object is deflected to the right in rotating frame of reference
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Coriolis force What is the sense of planetary rotation in the southern hemisphere? - Looking down onto the south pole, planetary rotation is clockwise Which direction would Coriolis force defect a moving particle in the southern hemisphere? - A moving object is deflected to the left in the southern hemisphere
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Latitudinal variation of Coriolis force Projecting the merry-go-round on the planet Parallel rotation axis at the pole Maximum Coriolis deflection Perpendicular rotation axis at the equator No Coriolis deflection
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General circulation (non-rotating atmosphere) Hadley cell Rising air at tropics Sinking air at poles Poleward flow in the upper atmosphere Equatorward flow in the lower atmosphere
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Hadley cell confined in low latitudes General circulation (rotating atmosphere) Rising air at tropics Sinking air at subtropics Equatorward flow deflected westwards (trade wind) Poleward flow deflected eastwards (westerly wind)
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Tank demo Hadley circulation: very low rotation rate (~ 1-2 RPM) “Pole” Low lat.
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Tank demo: Hadley cell Low-level trade wind Upper-level westerly wind
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Hadley cell dominates low-latitude circulation What controls the middle-high latitude circulation?
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Mid-latitude cyclones Weather system –Strong rotation effect generates turbulent motions –High and low pressures –Fronts: separating warm tropical air and cold polar airs
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Synoptic scale circulation High pressure Dry air sinking Sunny weather Air spirals out Clockwise Low pressure Moist air rising Rainy weather Air spirals in Counter-clockwise
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Tank demo Mid-latitude cyclones: high rotation rate (~ 5+ RPM) “Pole” Low lat.
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Tank demo Mid-latitude cyclones: high rotation rate (~ 5+ RPM)
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Putting it altogether “Hadley” regime Subtropical high Intertropical convergence zone (ITCZ) “Eddy” regime Variable weather Westerly wind
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